2b.7b Flashcards

1
Q

Define submergent coastline

A

sections of the littoral zone where sea level rise inundated areas that were previously part of terrestrial land

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2
Q

Define fossil cliff

A

a steep slope found at the back of a raised beach exhibiting evidence of formation through marine erosion but now above high tide level.

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3
Q

Define eustatic sea level rise

A

global sea-level changes related either to changes in the volume of glacial ice on land or to changes in the shape of the sea floor caused by plate tectonic processes

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4
Q

Explain eustatic (isostatic?..) sea level change as a result of tectonic activity

A

Faulting and folding of crust can create displacement of seabed (e.g. Sumatra since 2004 Earthquake, or Dalmatian coast in Croatia)

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5
Q

Explain eustatic sea level change as a result of post glacial period

A
  • Sea level rise approx. 125 m since the last Glacial Maximum (LGM) – 21,000 years ago!
  • Meltwater pulse around 14,000 years ago – most ice melted by 6,000 years ago and sea level is now only slowly rising.
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6
Q

What creates submergent coastlines

A

sea level changes

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7
Q

State three submergent coastline landforms

A

rias, fjords and dalmation coasts

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8
Q

What is a fjord

A

Submerged (flooded glaciated u shaped valley) U-shaped valley that has been over-deepened inland. Rock lip threshold exists at seaward entrance.

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9
Q

Where are fjords found?

A

Also found in Norway (e.g. Sognefjorden), New Zealand, Chile, Alaska, and Greenland.

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10
Q

What is a ria

A
  • Drowned (flooded river valley) valley due to river erosion (outside LGM ice extent) – e.g. Kingsbridge Estuary
  • dorwned by rising sea levels
  • Rivers eroded steep-sided V-shaped valleys into the frozen landscape giving the ria a V-shaped cross section when the valley flooded
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11
Q

Where are rias found

A

Also found SW Wales, Ireland (e.g. Cork), Brittany and NW Spain

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12
Q

State an example of a submergent coastline

A

Sognefjorden, Norway

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13
Q

Describe the fjord in norway

A

Largest Fjord system in Norway – extends 200 km inland from west coast
Alignment corresponds to fracture system in bedrock (exploited by rivers, then glaciers)
Main Fjord basin is at a depth of ~800m below present sea levels (although deepest point is 1308m bsl)
Entrance at seaward end is shallower (100-150m) due to a rock bar (threshold)

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14
Q

Define emergnet coastline

A

Emergent coastlines are being produced by post-glacial adjustment. These are parts of the littoral zone where a fall in sea level exposed land once part of the sea bed

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15
Q

State three characteristics of a raised beach

A
  • A relict beach now above high tide level
  • A flat surface covered by sand or rounded pebbles/boulders.
  • Usually vegetated by plant succession (though further succession prevented due to grazing)
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16
Q

Comapre shapes of rias and fjords

A
  • Rias have a sinuous plan profile reflecting the meandering river course. The plan view is dendritic as tributies are flooded by the rising sea.
  • Fjords often have a relatively straight profile as glaciers truncate spurs to produce a direct downslope route.
  • Glacier erosion is often cut deep into the landscape, often tens of metres lower than the adjacent unglaciated land - meaning that fjords are often deeper than the adjacent sea.
17
Q

Why do fjords and rias occur

A

Isostaic rebound - areas that were adjacent to glaciated areas sink down during marine transgression